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Bru
Bruosen is one of the few river harbours in the county. As landing place for the churchgoers, this place and the boatshed environment follow a tradition that goes back to the Middle Ages, but the country store of today is much younger.
Geitaknottane
Many travellers between Mundheim and Gjermundshamn are captivated by the expansive view toward Øynefjord, Varaldsøy and Folgefonna. The barren pine forest on the slopes on the upper-side of the road is not seen by many. Who would think that this area is home to rare species of plants and animals, creatures who have made their homes here for thousands of years?
Kvamskogen
The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.
Kyrping
The trading post down by the fjord at Kyrping does not belong to the oldest group of trading posts from the 1600s and 1700s. It was only after the liberalisation of the trading legislation that trade was established here.
Mundheim
At Mundheim there is a dangerous stretch of the highway. The mountainside has given way several times in this area. Typically, it happens in the spring, when the frost has loosened its grip.
Skånevik- the trading post
There are only two buildings left of the old trading and guesthouse settlement in Skånevik. They are in the centre, close to the main road passing through the settlement. The other buildings that belonged to the place, the lodging house (“Holteriet”), the bakery, the courthouse, the boathouse and the sea house with the store, were pulled down in the last century.
Stordalen
When the Etne water system was protected in 1994, preservation of the cultural landscape in Stordalen Valley was a a main objective. This is a valley with an exceptional abundance of Different types of plants and animals. In the grey alder forest in Stordalen there are more bird species than in most other places, in fact, denser than one tends to find in a tropical rainforest.
Vesoldo
Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.
